SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG

LI Jinyuan; LIU Jianmin; FANG Nianqiao; TANG Qichao; CAO Shugang; YAO Xinglong

doi:10.16028/j.1009-2722.2020.057

2020 Vol. 36, No. 10

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Article navigation > Marine Geology Frontiers > 2020 > 36(10): 84-92

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LI Jinyuan, LIU Jianmin, FANG Nianqiao, TANG Qichao, CAO Shugang, YAO Xinglong. SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG[J]. Marine Geology Frontiers, 2020, 36(10): 84-92. doi: 10.16028/j.1009-2722.2020.057

Citation:

LI Jinyuan, LIU Jianmin, FANG Nianqiao, TANG Qichao, CAO Shugang, YAO Xinglong. SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG[J]. Marine Geology Frontiers, 2020, 36(10): 84-92. doi: 10.16028/j.1009-2722.2020.057

SUBMARINE TOPOGRAPHY AND SEDIMENTARY CHARACTERISTICS OF OFFSHORE WIND FARM IN HEISHAN ISLAND OF SHANDONG

1.
Longyuan (Beijing) Wind Power Engineering Design Consulting Co., Ltd, Beijing 100083, China
2.
Hunan Longyuan Wind Power Co., Ltd, Changsha 410000, China
3.
School of Ocean Sciences, China University of Geosciences(Beijing), Beijing 100083, China

More Information

Corresponding author: LIU Jianmin, jianmin.liu.a@chnenergy.com.cn

Received Date: 20 May 2020

Publish Date: 28 October 2020

Abstract

Abstract

The sea area off the Shandong Peninsula is rich in wind resources and there are excellent conditions for large-scale development of wind energy. In order to understand the topography and sediment distribution patterns of the seabed, so as to promote the development of offshore wind farms smoothly, the sea area near the Heishan island was selected as a case for geological study. An integrated geological and geophysical survey was then undertaking in the selected area. The survey data suggests that the seafloor topography of the study area is rather gentle and the water depth changes from 10 m to 25 m, 17.5 m on average. The sediment in the study area is cyan gray, gray and light brown in color and dominated by silty sand which covers over 75% of the whole area. The kurtosis of the sediment varies from flat to medium to sharp. In the west part of the study area, the sorting of the seafloor sediment changes from 1.35 up to 1.80. while in the east part the sorting of the sea bottom sediment varies from 0.90 to 1.75. The mean grain size of bottom sediments of the whole study area ranges from 4.3Φ to 5.9 Φ and is silt dominated. The topography and sediment characteristics reflect that the study area is an area with weak hydrodynamic effect and therefore suitable for offshore wind power development and other kinds of sub-bottom constructions.
- Heishan Island /
- offshore wind farm /
- topographic features /
- type of bottom sediment /
- sedimentary characteristics /
- hydrodynamic environment

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References

[1]	孙雷,汪锋,张雯,等. 海上风电运维:从近海走向深远海域[J]. 太阳能,2018(6):6-10. Google Scholar
[2]	杨红生,茹小尚,张立斌,等. 海洋牧场与海上风电融合发展:理念与展望[J]. 中国科学院院刊,2019,34(6):700-707. Google Scholar
[3]	曾亮,储韬玉,王占华,等. 海上风电勘测中的物探技术[J]. 工程勘察,2019,47(7):66-72. Google Scholar
[4]	高抒,Collins M. 沉积物粒径趋势与海洋沉积动力学[J]. 中国科学基金,1998,12(4):241-246. Google Scholar
[5]	Ashley G M. Classification of large-scale subaqueous bedforms:a new look at an old problem[J]. Journal of Sedimentary Research,1990,60(1):160-172. doi: 10.2110/jsr.60.160 CrossRef Google Scholar
[6]	林纪江,胡日军,朱龙海,等. 潮流作用下蓬莱近岸海域悬浮泥沙的时空分布及变化特征[J]. 海洋地质前沿,2017,33(12):13-23. Google Scholar
[7]	中华人民共和国国家质量监督检疫总局. GB/T 12763.8-2007 海洋调查规范第8部分: 海洋地质地球物理调查[S]. 北京: 中国标准出版社, 2008. Google Scholar
[8]	McLaren P. An interpretation of trends in grain size measurements[J]. Journal of Sedimentary Petrology,1981,51:611-624. Google Scholar
[9]	Livingstone I,Wiggs G F S,Weaver C M. Geomorphology of desert sand dunes:a review of recent progress[J]. Earth-Science Reviews,2007,80(3/4):239-257. Google Scholar
[10]	左书华,韩志远,许婷. 烟台套子湾海域表层沉积物粒度分布特征及其动力响应[J]. 泥沙研究,2013(5):41-46. Google Scholar
[11]	陈燕萍,李琰. 舟山DZ-1钻孔沉积物粒度特征与沉积环境辨别[J]. 海洋学研究,2018,36(4):53-59. Google Scholar
[12]	刘春秀. 烟台近海海底表层沉积物粒度分布特征[D]. 青岛: 中国海洋大学, 2010. Google Scholar
[13]	Doeglas D J. Loess deposits of Mississippi. Krinitzsky E L,Turnbull W J.1967. Geological Society of America,Boulder,Colo. (Special Paper 94),64 pp.,U.S. $3.50[J]. Earth-Science Reviews,1968,4:71. Google Scholar
[14]	汤世凯,于剑峰,李金鹏,等. 烟台芝罘湾底质沉积物粒度特征和沉积动力环境研究[J]. 山东国土资源,2020,36(1):22-28. Google Scholar
[15]	贾海林,刘苍字,杨欧. 长江口北支沉积动力环境分析[J]. 华东师范大学学报(自然科学版),2001,1(1):90-96. Google Scholar
[16]	韦钦胜,于志刚,冉祥滨,等. 黄海西部沿岸流系特征分析及其对物质输运的影响[J]. 地球科学进展,2011,26(2):145-156. Google Scholar
[17]	张秀芝, 朱　蓉. 中国近海风电场开发指南[M]. 北京: 气象出版社, 2010: 60-61. Google Scholar
[18]	张　伟. 渤海海峡南部海域地貌特征及控制因素研究[D]. 青岛: 中国海洋大学, 2014. Google Scholar
[19]	Pejrup M. The triangular diagram used for classification of estuarine sediments: a new approach[M]//de Boer P L, van Gelder A, Nio S D. Tide-Influenced Sedimentary Environments and Facies. Netherlands: D. Reidel Publishing, 1988: 289-300. Google Scholar